哈塔伊省基里喀罕-库姆鲁地区土壤有用硼含量测定及其与土壤性质的关系

M. Yalçın
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引用次数: 0

摘要

本研究旨在测定哈塔伊省Kırıkhan-Kumlu地区土壤中有用硼含量及其与某些理化性质的关系。为此,总共从0-20和20-40 cm深度和30个不同的点采集了60个土壤样本来代表研究区域。测定了土壤的pH、总盐、组分、阳离子交换容量、石灰、有机质和有用硼含量。根据研究结果;土壤pH值为7.95 ~ 8.43;总含盐量0.009 ~ 0.115%;粘土含量18.88 ~ 74.16%;含砂量7.12 ~ 59.84%;含粉量15.28 ~ 52.72%;石灰含量0.47 ~ 26.59%;有机质含量1.16 ~ 6.08%;CEC含量22.26 ~ 72.83 me/100 g,有用硼含量0.10 ~ 1.25 mg/kg。哈塔伊省Kırıkhan-Kumlu土壤有效硼含量在0 ~ 20 cm深度为50.00%极低、40.00%低、10.00%充足,在20 ~ 40 cm深度为50.00%极低、43.34%低、6.66%充足。有效硼与土壤盐、粘土、石灰和CEC含量呈显著正相关,与土壤砂含量呈显著负相关。土壤中盐与粘土、石灰、CEC含量呈显著正相关,与pH、砂粒含量呈显著负相关。研究区土壤中粘土与有机质、CEC含量呈显著正相关,而粘土与砂土、粉土含量呈显著负相关。土壤有机质、CEC含量与沙粒呈显著负相关。同时,粉土与土壤CEC、石灰与土壤有机质含量呈显著负相关,有机质与土壤CEC呈显著正相关。结果表明,研究区所有土壤的有用硼含量均在92%以上的低水平和极低水平,表明土壤的有用硼含量不足,应进行硼施肥。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
DETERMINATION OF USEFUL BORON CONTENT OF THE SOILS OF KIRIKHAN-KUMLU REGION OF HATAY PROVINCE AND THEIR RELATIONSHIP WITH SOME SOIL PROPERTIES
In this study, it was aimed to determine the useful boron content of the soils of Kırıkhan-Kumlu region of Hatay province and its relationships with some physical and chemical properties. For this purpose, a total of 60 soil samples were taken from 0-20 and 20-40 cm depths and from 30 different points to represent the study area. The pH, total salt, composition, cation exchange capacity (CEC), lime, organic matter and useful boron contents of the soils were determined. According to the results of the research; pH contents of the soils were 7.95-8.43; total salt contents 0.009-0.115 %; clay contents 18.88-74.16 %; sand contents 7.12-59.84 %; silt contents 15.28-52.72 %; lime contents 0.47-26.59 %; organic matter contents 1.16-6.08 %; CEC contents 22.26-72.83 me/100 g and useful boron contents 0.10-1.25 mg/kg. In terms of useful boron content of Kırıkhan-Kumlu soils of Hatay province, it was determined that 50.00 % of them were very low, 40.00 % were low and 10.00 % were sufficient at 0-20 cm depth and 50.00 % of them were very low, 43.34 % were low and 6.66 % were sufficient at 20-40 cm depth. While a positive significant relationship was determined between useful boron and salt, clay, lime and CEC contents of soils, a negative significant relationship was determined between useful boron and sand content. Positive significant relationships were determined between salt and clay, lime and CEC contents of the soils, while negative significant relationships were determined between salt and pH and sand contents. Positive significant relationships were determined between clay and organic matter and CEC contents of the study area soils, while negative significant relationships were determined between clay and sand and silt contents. Significant negative relationships were determined between sand and organic matter and CEC contents of the soils. At the same time, while negative significant relationships were determined between silt and CEC and lime and organic matter contents of the soils, positive significant relationships were determined between organic matter and CEC. As a result, it was seen that the useful boron content of the soils in the study area was determined at low and very low levels above 92 % in all soils of the study area and it was seen that the useful boron content of the soils was insufficient and therefore boron fertilization should be done.
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